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Table of Contents
Vocabulary
Outline
T= Volcanic Activity
How Magma Reaches Earth's Surface
Magma Rises
A Volcano Erupts
Inside a Volcano
Characteristics of the Magma
Types of Volcanic Eruptions
Quiet Eruptions
Explosive Eruptions
To go back to the Teamforce Homepage, click
here
To go back to the GWBN Homepage, click
here
Vocabulary
magma chamber-
a pocket in which magma collects
pipe-
a long tube in the ground that connects the magma chamber to the Earth's surface
vent-
an opening where molten rock and gas leave
lava flow-
an area covered by lava as it pours out of a vent
crater-
a bowl shaped area that may form at the top of a volcano around the volcano's central vent
Silica-
a material that is formed from elements oxygen and silicon
Pahoehoe-
fast moving, hot lava
aa-
cooler, slower moving lava
pyroclastic flow-
occurs when explosive eruption hurls out ash, cinders, bombs and gases
active-
the term for a live volcano, having the ability to erupt in the near future
dormant-
a 'sleeping' volcano, opposite of active, may be able to erupt in the future
extinct
- a dead volcano, which is unlikely to erupt again
hot spring-
formed when groundwater heated by nearby body of magma rises to the surface and collects in a natural pool
geothermal energy-
water heated by magma produces this clean energy
Outline
T= Volcanic Activity
How Magma Reaches Earth's Surface
lava begins as magma
magma forms in asthenosphere
materials of asthenosphere under great pressure
Magma Rises
liquid magma is less dense than surrounding solid material, it flow upward into cracks
magma floats up until trapped or reaches the surface
A Volcano Erupts
dissolved gases trapped in magma under tremendous pressure
as magma rises toward the surface, pressure decreases
volcano erupts when opening develops in weak rock
once magma reaches surface, becomes lava and gases bubble out
Inside a Volcano
beneath a volcano, magma collects in magma chamber
magma moves through a pipe
molten rock and gases leave the volcano through a vent
Characteristics of the Magma
the force of a volcanic eruption depends on
gas content of magma
thickness of magma
how much silica the magma contains
Types of Volcanic Eruptions
The silica content in magma helps determine whether the eruption is quiet or explosive
Quiet Eruptions
a volcano erupts if the magma flows easily
Quiet Eruptions produce two eruptions=
Pahoehoe
fast moving, hot lava
surface of lava looks like rope- like coils
aa
when hardens, it forms a rough, jagged chunks of lava
Explosive Eruptions
If thick and sticky, the magma will erupt explosively
the pressure will build until it explodes
hurtles out=
bombs
fine sand grains
pyroclastic flow
To go back to the top, click
here
A diagram of a volcano
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Table of Contents
To go back to the Teamforce Homepage, click hereTo go back to the GWBN Homepage, click here
Vocabulary
magma chamber- a pocket in which magma collects
pipe- a long tube in the ground that connects the magma chamber to the Earth's surface
vent- an opening where molten rock and gas leave
lava flow- an area covered by lava as it pours out of a vent
crater- a bowl shaped area that may form at the top of a volcano around the volcano's central vent
Silica- a material that is formed from elements oxygen and silicon
Pahoehoe- fast moving, hot lava
aa- cooler, slower moving lava
pyroclastic flow- occurs when explosive eruption hurls out ash, cinders, bombs and gases
active- the term for a live volcano, having the ability to erupt in the near future
dormant- a 'sleeping' volcano, opposite of active, may be able to erupt in the future
extinct- a dead volcano, which is unlikely to erupt again
hot spring- formed when groundwater heated by nearby body of magma rises to the surface and collects in a natural pool
geothermal energy- water heated by magma produces this clean energy
Outline
T= Volcanic Activity
- lava begins as magma
- magma forms in asthenosphere
- materials of asthenosphere under great pressure
- liquid magma is less dense than surrounding solid material, it flow upward into cracks
- magma floats up until trapped or reaches the surface
- dissolved gases trapped in magma under tremendous pressure
- as magma rises toward the surface, pressure decreases
- volcano erupts when opening develops in weak rock
- once magma reaches surface, becomes lava and gases bubble out
- beneath a volcano, magma collects in magma chamber
- magma moves through a pipe
- molten rock and gases leave the volcano through a vent
- the force of a volcanic eruption depends on
- gas content of magma
- thickness of magma
- how much silica the magma contains
- The silica content in magma helps determine whether the eruption is quiet or explosive
- a volcano erupts if the magma flows easily
- Quiet Eruptions produce two eruptions=
- Pahoehoe
- fast moving, hot lava
- surface of lava looks like rope- like coils
- aa
- when hardens, it forms a rough, jagged chunks of lava
- If thick and sticky, the magma will erupt explosively
- the pressure will build until it explodes
- hurtles out=
- bombs
- fine sand grains
- pyroclastic flow
To go back to the top, click hereHow Magma Reaches Earth's Surface
Magma Rises
A Volcano Erupts
Inside a Volcano
Characteristics of the Magma
Types of Volcanic Eruptions
Quiet Eruptions
Explosive Eruptions